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land, including its relief, landforms and overall appearance."},{"text":"rock type and structure","correct":false,"explanation":"Rock type and structure influence landscapes, but the visible feature being defined is their shape and character, which describes the land’s overall appearance."},{"text":"height and steepness","correct":false,"explanation":"Height and steepness are important aspects of relief, but the broader definition of a physical landscape is the visible shape and character of the land."},{"text":"vegetation and wildlife","correct":false,"explanation":"Vegetation and wildlife are parts of the natural environment, not the definition of a physical landscape, which is the visible shape and character of the land."}]},{"id":"eaabc623-839c-4169-9c7a-0e1422c625f5","cardType":"cloze","points":null,"front":"[ ] are higher, steeper and often have thinner soils; [ ] are lower, flatter and often have deeper soils.","back":"Uplands are higher, steeper and often have thinner soils; lowlands are lower, flatter and often have deeper soils.","mcqOptions":[{"text":"Uplands are higher, steeper and often have thinner soils; lowlands are lower, flatter and often have deeper soils.","correct":true,"explanation":"Uplands generally have greater elevation and steeper slopes, with thinner soils, while lowlands are flatter and commonly have deeper soils."},{"text":"Lowlands are higher, steeper and often have thinner soils; uplands are lower, flatter and often have deeper soils.","correct":false,"explanation":"The descriptions have been reversed: uplands are higher and steeper, whereas lowlands are lower and flatter, often with deeper soils."},{"text":"Uplands are lower, flatter and often have deeper soils; lowlands are higher, steeper and often have thinner soils.","correct":false,"explanation":"This option assigns lowland characteristics to uplands and vice versa. Uplands are higher, steeper and thinner-soiled; lowlands are lower, flatter and deeper-soiled."},{"text":"Uplands are higher, flatter and often have deeper soils; lowlands are lower, steeper and often have thinner soils.","correct":false,"explanation":"The elevation is correct, but the slope and soil characteristics are not. Uplands are usually steeper with thinner soils, while lowlands are flatter with deeper soils."}]},{"id":"746b3b19-7f03-4774-953d-ae271626b4fa","cardType":"cloze","points":null,"front":"UK uplands are mostly in the [ ]; lowlands are more common in the [ ].","back":"UK uplands are mostly in the north and west; lowlands are more common in the south and east.","mcqOptions":[{"text":"UK uplands are mostly in the north and west; lowlands are more common in the south and east.","correct":true,"explanation":"The UK’s main upland areas are concentrated in the north and west, while lower and flatter landscapes are more widespread in the south and east."},{"text":"UK uplands are mostly in the south and east; lowlands are more common in the north and west.","correct":false,"explanation":"The regions have been reversed. Uplands are mainly found in the north and west, whereas lowlands are more common in the south and east."},{"text":"UK uplands are mostly in the north and east; lowlands are more common in the south and west.","correct":false,"explanation":"The north is associated with uplands, but the key pattern is north and west. Lowlands are more common in the south and east, not the south and west."},{"text":"UK uplands are mostly in the south and west; lowlands are more common in the north and east.","correct":false,"explanation":"Although some upland areas occur in the west, the overall distribution is north and west for uplands and south and east for lowlands."}]},{"id":"059f1616-4dc1-4f8d-838f-59024d158589","cardType":"basic","points":2,"front":"Why do less resistant rocks often form lower, gentler landscapes?","back":"They are worn away more easily by erosion and weathering.","mcqOptions":[{"text":"They are worn away more easily by erosion and weathering.","correct":true,"explanation":"Less resistant rocks break down and are removed more easily by weathering and erosion, leaving lower elevations and gentler slopes over time."},{"text":"They are lifted up more quickly by tectonic forces and weathering.","correct":false,"explanation":"Tectonic uplift can raise land, but it does not explain why less resistant rocks form lower, gentler landscapes. They are worn away more easily by erosion and weathering."},{"text":"They are deposited more rapidly by rivers and glaciers.","correct":false,"explanation":"Deposition can build areas up, but the key process affecting less resistant rocks is their faster removal. They are worn away more easily by erosion and weathering."},{"text":"They are heated and compressed more strongly beneath the surface.","correct":false,"explanation":"Heat and pressure can alter rocks, but they do not directly explain the lower, gentler relief. Less resistant rocks are worn away more easily by erosion and weathering."}]},{"id":"14ab4794-2132-46f2-8950-b5029dd11cc2","cardType":"cloze","points":null,"front":"Sedimentary rocks form when layers of [ ] are [ ] over time.","back":"Sedimentary rocks form when layers of sediment are compacted and cemented over time.","mcqOptions":[{"text":"Sedimentary rocks form when layers of sediment are compacted and cemented over time.","correct":true,"explanation":"Sedimentary rocks develop from deposited sediment. Burial compacts the layers, while minerals cement the particles together over a long period."},{"text":"Sedimentary rocks form when layers of magma are cooled and solidified over time.","correct":false,"explanation":"Cooling and solidification of magma forms igneous rock. Sedimentary rock forms when layers of sediment are compacted and cemented over time."},{"text":"Sedimentary rocks form when layers of sediment are heated and melted over time.","correct":false,"explanation":"Heating and melting do not produce sedimentary rock and would destroy the original layers. Sediment becomes sedimentary rock through compaction and cementation."},{"text":"Sedimentary rocks form when layers of existing rock are folded and uplifted over time.","correct":false,"explanation":"Folding and uplift are tectonic processes, not the main formation process for sedimentary rocks. Layers of sediment must be compacted and cemented over time."}]},{"id":"82f3cfec-1f17-443f-86b1-921c00a26bc1","cardType":"cloze","points":null,"front":"Igneous rocks form when [ ] [ ].","back":"Igneous rocks form when molten rock cools and solidifies.","mcqOptions":[{"text":"Igneous rocks form when molten rock cools and solidifies.","correct":true,"explanation":"Igneous rocks form as molten rock cools and changes from a liquid state into solid crystals, either below ground or at the surface."},{"text":"Igneous rocks form when sediment is compacted and cemented.","correct":false,"explanation":"Compaction and cementation form sedimentary rocks. Igneous rocks form when molten rock cools and solidifies."},{"text":"Igneous rocks form when existing rock is changed by heat and pressure.","correct":false,"explanation":"Heat and pressure changing existing rock describes metamorphic rock formation. Igneous rocks form when molten rock cools and solidifies."},{"text":"Igneous rocks form when weathered material is deposited in layers.","correct":false,"explanation":"Deposited weathered material can eventually form sedimentary rock, not igneous rock. Igneous rocks form from molten rock that cools and solidifies."}]},{"id":"46bb5d16-0f4e-4ec5-a851-9c465d9b5558","cardType":"basic","points":2,"front":"Why do igneous rocks often help form rugged uplands?","back":"They are usually resistant to erosion and weathering.","mcqOptions":[{"text":"They are usually resistant to erosion and weathering.","correct":true,"explanation":"Igneous rocks are often hard and resistant, so erosion and weathering remove them slowly. This allows steep slopes and rugged upland landscapes to remain."},{"text":"They are usually weak against erosion and weathering.","correct":false,"explanation":"Weak rocks are removed more easily and tend to form lower, gentler landscapes. Igneous rocks often create rugged uplands because they are resistant to erosion and weathering."},{"text":"They are usually formed from deep soils by erosion and weathering.","correct":false,"explanation":"Soil formation does not explain the resistance of igneous rocks. Their rugged uplands result because the rocks are usually resistant to erosion and weathering."},{"text":"They are usually deposited in loose layers by rivers and weathering.","correct":false,"explanation":"Loose deposited layers are more typical of sedimentary material and are vulnerable to erosion. Igneous rocks often form rugged uplands because they resist erosion and weathering."}]},{"id":"2f6ef445-ae17-4924-9b83-9ce8920d8bb0","cardType":"cloze","points":null,"front":"Metamorphic rocks form when existing rocks are changed by [ ] and [ ].","back":"Metamorphic rocks form when existing rocks are changed by heat and pressure.","mcqOptions":[{"text":"Metamorphic rocks form when existing rocks are changed by heat and pressure.","correct":true,"explanation":"Metamorphic rocks are existing rocks altered deep underground by heat and pressure, without completely melting into magma."},{"text":"Metamorphic rocks form when existing rocks are changed by cooling and solidification.","correct":false,"explanation":"Cooling and solidification form igneous rocks from molten material. Metamorphic rocks form when existing rocks are altered by heat and pressure."},{"text":"Metamorphic rocks form when existing rocks are changed by weathering and deposition.","correct":false,"explanation":"Weathering and deposition contribute to sedimentary rock formation, not metamorphism. Metamorphic rocks are changed by heat and pressure."},{"text":"Metamorphic rocks form when existing rocks are changed by erosion and cementation.","correct":false,"explanation":"Cementation helps form sedimentary rocks from sediment, while erosion removes material. Metamorphic rocks form when existing rocks are changed by heat and pressure."}]},{"id":"1deb5b80-3007-484b-bd15-d63ce25699ed","cardType":"basic","points":3,"front":"What is the simple UK rock distribution pattern?","back":"

Older igneous and metamorphic rocks - north and west uplands.
Younger sedimentary rocks - south and east lowlands.

","mcqOptions":[{"text":"

Older igneous and metamorphic rocks - north and west uplands.
Younger sedimentary rocks - south and east lowlands.

","correct":true,"explanation":"This is the simple pattern: resistant older igneous and metamorphic rocks are concentrated in the north and west, while younger sedimentary rocks generally form the south and east lowlands."},{"text":"

Younger sedimentary rocks - north and west uplands.
Older igneous and metamorphic rocks - south and east lowlands.

","correct":false,"explanation":"This reverses the broad UK pattern. Older igneous and metamorphic rocks are mainly found in the north and west uplands, whereas younger sedimentary rocks dominate the south and east lowlands."},{"text":"

Older sedimentary rocks - north and west uplands.
Younger igneous and metamorphic rocks - south and east lowlands.

","correct":false,"explanation":"The rock types have been wrongly assigned and their ages have been reversed. The broad pattern is older igneous and metamorphic rocks in northern and western uplands, with younger sedimentary rocks in the south and east."},{"text":"

Younger igneous and metamorphic rocks - north and west uplands.
Older sedimentary rocks - south and east lowlands.

","correct":false,"explanation":"This combines two common errors by reversing both rock age and rock type. UK uplands generally contain older igneous and metamorphic rocks, while the lowlands mainly contain younger sedimentary rocks."}]},{"id":"a768710d-4f3e-4cc0-b5be-b48f8e97229c","cardType":"basic","points":2,"front":"Why is 'all uplands are igneous' an overgeneralisation?","back":"The Pennines are upland but include resistant sedimentary rocks.","mcqOptions":[{"text":"The Pennines are upland but include resistant sedimentary rocks.","correct":true,"explanation":"The Pennines show why the generalisation fails: they are upland areas formed partly from resistant sedimentary rocks, not exclusively from igneous rocks."},{"text":"The Lake District is lowland but includes resistant sedimentary rocks.","correct":false,"explanation":"The Lake District is an upland area, so changing it to lowland makes this explanation wrong. The key example is the Pennines, which are upland but include resistant sedimentary rocks."},{"text":"The Pennines are upland but include soft sedimentary rocks.","correct":false,"explanation":"The Pennines are the correct example, but resistant rocks help form upland relief; describing these sedimentary rocks as soft reverses the relevant geological explanation."},{"text":"The Pennines are lowland but include resistant sedimentary rocks.","correct":false,"explanation":"The rock description is relevant, but the Pennines are upland rather than lowland. Their upland character demonstrates that resistant sedimentary rocks can occur in upland landscapes."}]},{"id":"ca3dd8e3-81d9-414e-9f8a-23866a0f21f6","cardType":"basic","points":2,"front":"How did ancient tectonic activity help create some UK uplands?","back":"It uplifted, folded or faulted rocks, raising some resistant areas.","mcqOptions":[{"text":"It uplifted, folded or faulted rocks, raising some resistant areas.","correct":true,"explanation":"Ancient tectonic forces deformed the UK's rocks through uplift, folding and faulting. This raised some areas and helped resistant rocks form upland landscapes."},{"text":"It weathered, eroded or deposited rocks, lowering some resistant areas.","correct":false,"explanation":"These are mainly surface processes and the stated effect is reversed. Ancient tectonic activity uplifted, folded or faulted rocks, raising some resistant areas to form uplands."},{"text":"It melted, cooled or crystallised rocks, creating all UK uplands.","correct":false,"explanation":"Melting, cooling and crystallisation describe igneous processes, not the main tectonic explanation here. Tectonic activity uplifted, folded or faulted rocks, and it did not create all UK uplands."},{"text":"It transported, deposited or compacted rocks, raising all lowlands.","correct":false,"explanation":"Transport, deposition and compaction are sedimentary or surface processes, not the relevant tectonic mechanism. Ancient tectonic activity uplifted, folded or faulted rocks, raising some resistant areas."}]},{"id":"ba2377d1-dc23-43a2-a4e1-366639dbd759","cardType":"basic","points":1,"front":"What effect can glacial erosion have on upland valleys?","back":"It can deepen valleys.","mcqOptions":[{"text":"It can deepen valleys.","correct":true,"explanation":"Glaciers erode the floors and sides of existing valleys, often changing narrow V-shaped valleys into deeper, wider U-shaped valleys."},{"text":"It can shallow valleys.","correct":false,"explanation":"Glacial erosion removes material from valley floors and sides, so it generally deepens and widens valleys rather than making them shallower."},{"text":"It can fill valleys.","correct":false,"explanation":"Filling valleys is associated with deposition, such as sediment left by ice or meltwater. Glacial erosion instead removes rock and can deepen valleys."},{"text":"It can straighten rivers.","correct":false,"explanation":"Glacial erosion reshapes valley profiles rather than primarily straightening rivers. Its characteristic effect on upland valleys is to deepen and widen them into U-shaped forms."}]},{"id":"f6228d46-a05c-40a7-bc4d-9532a7d7fa06","cardType":"basic","points":1,"front":"Name one deposit left by glacial deposition.","back":"A moraine (also till or a drumlin).","mcqOptions":[{"text":"A moraine (also till or a drumlin).","correct":true,"explanation":"Moraines, till and drumlins are glacial deposits or landforms created when glaciers deposit material. A moraine is therefore a valid example of glacial deposition."},{"text":"A delta.","correct":false,"explanation":"A delta forms where a river deposits sediment at its mouth, not directly through glacial deposition. A moraine, till or drumlin would be a correct glacial example."},{"text":"An oxbow lake.","correct":false,"explanation":"An oxbow lake forms when a meander is cut off from a river channel. It is a fluvial feature, whereas a moraine, till or drumlin is linked to glacial deposition."},{"text":"A levee.","correct":false,"explanation":"A levee is a raised river bank formed by flood deposition, so it is associated with fluvial processes. Glacial deposition produces features such as moraines, till and drumlins."}]},{"id":"d7e741cd-0c10-4290-a6ac-014228b0fb9c","cardType":"cloze","points":null,"front":"Weathering breaks rock down [ ]; erosion wears away and [ ].","back":"Weathering breaks rock down in place; erosion wears away and removes material.","mcqOptions":[{"text":"Weathering breaks rock down in place; erosion wears away and removes material.","correct":true,"explanation":"Weathering breaks rock down where it is, without transporting it. Erosion involves wearing material away and removing it, usually through moving water, ice, wind or waves."},{"text":"Weathering breaks rock down through heat; erosion wears away and creates material.","correct":false,"explanation":"Heat can contribute to some weathering, but the defining contrast is location: weathering occurs in place, while erosion wears away and removes material rather than creating it."},{"text":"Weathering breaks rock down by transport; erosion wears away and leaves material.","correct":false,"explanation":"Transport is associated with erosion, not weathering, and erosion does not simply leave material behind. Weathering acts in place, while erosion wears away and removes material."},{"text":"Weathering breaks rock down into soil layers; erosion wears away and deposits material.","correct":false,"explanation":"Weathering does not always produce soil layers, and deposition is the settling of transported material rather than the definition of erosion. The correct distinction is breakdown in place versus removal."}]},{"id":"3e2c021d-c18d-4e39-906d-d62911a897f4","cardType":"basic","points":2,"front":"How does freeze-thaw weathering force rock apart?","back":"

Water enters cracks in the rock.
Freezing expansion forces the rock apart.

","mcqOptions":[{"text":"

Water enters cracks in the rock.
Freezing expansion forces the rock apart.

","correct":true,"explanation":"Water enters cracks, then expands when it freezes. Repeated freezing and thawing widens the cracks until pieces of rock are forced apart."},{"text":"

Water evaporates from cracks in the rock.
Cooling contraction forces the rock apart.

","correct":false,"explanation":"Evaporation and contraction do not explain freeze-thaw weathering. Water enters cracks and expands on freezing, exerting pressure that forces the rock apart."},{"text":"

Salt enters cracks in the rock.
Freezing expansion forces the rock apart.

","correct":false,"explanation":"Freezing expansion is the relevant force, but the process begins with water entering cracks. Replacing water with salt confuses freeze-thaw weathering with salt crystallisation."},{"text":"

Water enters cracks in the rock.
Melting contraction forces the rock apart.

","correct":false,"explanation":"Water entering cracks is correct, but melting causes ice to contract rather than expand. It is the expansion of freezing water that creates pressure and breaks the rock."}]},{"id":"76788ca0-edd2-46ab-932a-9b7c69147e08","cardType":"basic","points":2,"front":"What climate conditions help explain thin soils and fast streams in north and west uplands?","back":"They are generally wetter and more exposed.","mcqOptions":[{"text":"They are generally wetter and more exposed.","correct":true,"explanation":"North and west uplands receive more rainfall and are more exposed to wind. Wetter conditions can increase leaching, while exposure and steep slopes encourage fast-flowing streams and thin soils."},{"text":"They are generally drier and more sheltered.","correct":false,"explanation":"This reverses the typical upland climate. North and west uplands are generally wetter and more exposed, helping explain leached thin soils and rapidly flowing streams."},{"text":"They are generally warmer and less exposed.","correct":false,"explanation":"Uplands are usually cooler and more exposed than lowlands, not warmer and sheltered. The relevant conditions in the north and west are wetter weather and greater exposure."},{"text":"They are generally hotter and more humid.","correct":false,"explanation":"Greater humidity alone does not explain the pattern, and uplands are not generally hotter. Wetter, more exposed conditions promote thin soils and fast streams in these areas."}]},{"id":"0200a384-959a-41d9-91b3-ffe937a012c0","cardType":"basic","points":1,"front":"Where do rivers commonly deposit material in lowlands?","back":"On floodplains.","mcqOptions":[{"text":"On floodplains.","correct":true,"explanation":"River velocity often falls when water spreads across low-lying land, so the river loses energy and deposits sediment on its floodplain."},{"text":"On river cliffs.","correct":false,"explanation":"River cliffs form on the outside of meanders, where faster flow causes erosion rather than deposition. In lowlands, deposition commonly occurs on floodplains."},{"text":"On watersheds.","correct":false,"explanation":"Watersheds are ridges separating drainage basins and are not lowland depositional features. Rivers commonly deposit material on floodplains as their velocity and energy decrease."},{"text":"On interlocking spurs.","correct":false,"explanation":"Interlocking spurs are upland landforms associated with river erosion in youthful valleys. In lowlands, rivers commonly deposit sediment on floodplains."}]},{"id":"df9b1126-d31d-40ee-85a2-4686fbffe8c9","cardType":"basic","points":1,"front":"What force drives slope processes such as soil creep, landslides and rockfalls?","back":"Gravity.","mcqOptions":[{"text":"Gravity.","correct":true,"explanation":"Gravity pulls weathered material downhill, driving mass-movement processes including soil creep, landslides and rockfalls."},{"text":"Hydraulic action.","correct":false,"explanation":"Hydraulic action is erosion caused by the force of moving water, not the force driving material down slopes. Slope processes are driven by gravity."},{"text":"Friction.","correct":false,"explanation":"Friction usually resists the downhill movement of material rather than driving it. Gravity supplies the force responsible for soil creep, landslides and rockfalls."},{"text":"Wind.","correct":false,"explanation":"Wind can transport exposed sediment, but it does not drive the main mass-movement processes listed. Gravity pulls soil and rock downhill."}]},{"id":"6911a6d1-e566-4945-a953-f830cb6c856f","cardType":"basic","points":2,"front":"Why is sheep grazing common in UK uplands?","back":"Steep slopes, thin soils and harsher weather limit other farming.","mcqOptions":[{"text":"Steep slopes, thin soils and harsher weather limit other farming.","correct":true,"explanation":"UK uplands often have steep terrain, shallow soils and severe weather, making crop cultivation difficult while hardy sheep can graze there."},{"text":"Flat slopes, deep soils and milder weather limit other farming.","correct":false,"explanation":"Deep soils, flat land and mild weather favour arable cultivation rather than explaining upland sheep grazing. Steep slopes, thin soils and harsher weather limit other farming."},{"text":"Fertile soils, warm summers and longer seasons limit other farming.","correct":false,"explanation":"Fertile soils and long growing seasons would support crops, not restrict other types of farming. Upland grazing reflects steep slopes, thin soils and harsher weather."},{"text":"Dense settlement, busy roads and extensive railways limit other farming.","correct":false,"explanation":"Dense settlement and extensive transport links are more characteristic of accessible lowlands and do not explain sheep grazing. Upland farming is constrained by steep slopes, thin soils and harsher weather."}]},{"id":"9c4db9a5-5e4d-47e1-a3cb-1f619158ed42","cardType":"basic","points":2,"front":"Why is arable farming more common in lowlands?","back":"Deeper soils and flatter land make farming easier.","mcqOptions":[{"text":"Deeper soils and flatter land make farming easier.","correct":true,"explanation":"Lowlands generally provide deeper, more workable soils and level ground, allowing machinery to operate efficiently and crops to be cultivated more easily."},{"text":"Thinner soils and steeper land make farming easier.","correct":false,"explanation":"Thin soils and steep slopes make machinery and crop cultivation more difficult, so they characterise upland constraints. Deeper soils and flatter land favour arable farming."},{"text":"Rockier soils and waterlogged land make farming easier.","correct":false,"explanation":"Rocky soils obstruct cultivation, while waterlogged land can deprive crop roots of oxygen. Arable farming is favoured by deeper soils and flatter land."},{"text":"Harsher weather and shorter seasons make farming easier.","correct":false,"explanation":"Harsher weather and shorter growing seasons restrict crop growth and are associated more strongly with uplands. Deeper soils and flatter land make lowland farming easier."}]},{"id":"589ff6b5-f322-44f0-b937-fa7b64099c6e","cardType":"basic","points":2,"front":"Why are conifer plantations often found in uplands?","back":"Upland land is less suitable for crops or dense settlement.","mcqOptions":[{"text":"Upland land is less suitable for crops or dense settlement.","correct":true,"explanation":"Because uplands are difficult to cultivate and build on, forestry can use land that has fewer competing demands from arable farming or major settlements."},{"text":"Upland land is more suitable for crops and dense settlement.","correct":false,"explanation":"Land well suited to intensive crops and dense settlement has high competing demand and is unlikely to be devoted to plantations. Upland land is generally less suitable for these uses."},{"text":"Upland land has deeper soils for intensive arable farming.","correct":false,"explanation":"Uplands commonly have thin, acidic soils rather than deep, highly fertile ones. Conifer plantations occur because this land is less suitable for crops or dense settlement."},{"text":"Upland land has flatter terrain for roads and housing.","correct":false,"explanation":"Gentle terrain and easy transport access are more typical advantages of lowlands. Upland forestry uses land that is less suitable for crops or dense settlement."}]},{"id":"e6836e32-ca0c-4274-aee9-e526b769ab59","cardType":"basic","points":2,"front":"Why do lowlands usually have more settlements?","back":"Flatter land is easier to build on, travel across and farm.","mcqOptions":[{"text":"Flatter land is easier to build on, travel across and farm.","correct":true,"explanation":"Level terrain reduces the difficulty and cost of construction, transport and cultivation, so lowland areas can support larger and more numerous settlements."},{"text":"Steeper land is easier to build on, travel across and farm.","correct":false,"explanation":"Steeper land makes construction, transport and mechanised farming more difficult and expensive. Lowland settlement is encouraged by flatter land."},{"text":"Rockier land is easier to build on, travel across and farm.","correct":false,"explanation":"Rockier land hinders foundations, road construction and cultivation rather than making them easier. Lowlands attract settlement because their terrain is flatter."},{"text":"Waterlogged land is easier to build on, travel across and farm.","correct":false,"explanation":"Waterlogged land creates unstable foundations and restricts transport and farming, so it does not explain settlement concentration. Flatter land provides the main accessibility advantage."}]},{"id":"24ff847c-36ca-4d44-ab5d-c5856715353b","cardType":"cloze","points":null,"front":"On OS maps, [ ] show steep slopes; [ ] show gentle slopes.","back":"On OS maps, close contours show steep slopes; widely spaced contours show gentle slopes.","mcqOptions":[{"text":"On OS maps, close contours show steep slopes; widely spaced contours show gentle slopes.","correct":true,"explanation":"Contours join points of equal elevation. Rapid height change over a short horizontal distance produces close contours, while gradual height change produces widely spaced contours."},{"text":"On OS maps, widely spaced contours show steep slopes; close contours show gentle slopes.","correct":false,"explanation":"This reverses the contour-spacing rule. Close contours indicate elevation changing rapidly over a short distance, so they show steep slopes; widely spaced contours show gentle slopes."},{"text":"On OS maps, close contours show steep slopes; contours crossing rivers show gentle slopes.","correct":false,"explanation":"Close contours correctly indicate steep slopes, but contours crossing rivers do not define gentle slopes. Gentle slopes are represented by widely spaced contours."},{"text":"On OS maps, index contours show steep slopes; widely spaced contours show gentle slopes.","correct":false,"explanation":"Index contours are simply emphasised and labelled contour lines, so they do not necessarily indicate steepness. Close contours show steep slopes, while widely spaced contours show gentle slopes."}]},{"id":"41fae357-fad3-4086-b602-fd4814d6baec","cardType":"basic","points":2,"front":"On a 1:50,000 OS map, two points are 4 cm apart. What is the real straight-line distance?","back":"2 km.","mcqOptions":[{"text":"2 km.","correct":true,"explanation":"At 1:50,000, 1 cm represents 50,000 cm, or 0.5 km. Therefore, 4 cm represents $4 \\times 0.5 = 2$ km."},{"text":"20 km.","correct":false,"explanation":"This results from treating 1 cm as 5 km, introducing a factor-of-ten conversion error. At 1:50,000, 1 cm is 0.5 km, giving 2 km."},{"text":"0.2 km.","correct":false,"explanation":"This divides by an extra factor of ten when converting the map measurement. Since each centimetre represents 0.5 km, 4 cm represents 2 km."},{"text":"200 km.","correct":false,"explanation":"This treats centimetres as kilometres without correctly converting 50,000 cm into 0.5 km. Multiplying 4 cm by 0.5 km per centimetre gives 2 km."}]}]}],"examCountdown":{"examDate":"2027-05-18","paperLabel":"Paper 1"},"heading":"Overview of the UK's physical landscape","title":"Overview of the UK's physical landscape Flashcards","topbar":{"backHref":"/gcse/geography/edexcel/a/flashcards"},"topicSidebar":"$L39"}]}],"topicId":"9e4b0681-9833-589c-a4e2-00748e17fb04","walled":"$L3a"}],"$L3b","$L3c"]